Abstract
The essential steps of photosynthetic water splitting take place in Photosystem II (PS II) and comprise three different reaction sequences: (i) light induced formation of the radical pair P680 + Q A - , (ii) P680 + driven oxidative water splitting into O 2 and four protons, and (iii) two step plastoquinone reduction to plastoquinol by Q A - . This mini-review briefly summarizes our state of knowledge on energetics, kinetics and mechanism of oxidative water splitting. Essential features of the two types of reactions involved are described: (a) P680 + reduction by the redox active tyrosine Y z and (b) sequence of oxidation steps induced by Y z ox in the water-oxidizing complex (WOC). The rate of the former reaction is limited by the non-adiabatic electron transfer (NET) step and the multi-phase kinetics shown to originate from a sequence of relaxation processes. In marked contrast, the rate of the stepwise oxidation by Y z ox of the WOC up to the redox level S 3 is not limited by NET but by trigger reactions which probably comprise proton shifts and/or conformational changes. The overall rate of the final reaction sequence leading to formation and release of O 2 is assumed to be limited by the electron transfer step from the S 3 state of WOC to Y z ox due to involvement of an endergonic redox equilibrium. Currently discussed controversial ideas on possible pathways are briefly outlined. Several crucial points of the mechanism of oxidative water splitting, like O–O bond formation, role of local proton shift(s), details of hydrogen bonding, are still not clarified and remain a challenging topic of future research.
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